Holocene Epoch Current Affairs
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Scientists have approved three new ages on geologic time scale of Holocene Epoch viz. Meghalayan Age, Middle Holocene Northgrippian Age and Early Holocene Greenlandian Age. These three new ages of Holocene Epoch are represented by wealth of sediments that accumulated worldwide on sea floor, on lake bottoms, as glacial ice, and as calcite layers in stalactites and stalagmites.Together the strata of three new stages comprise the Holocene series.
Meghalayan Age: It is named after cave in Indian state of Meghalaya. It has helped to define climatic events 4,200 years ago, marking beginning of phase that continues till today. The lower boundary of this stage is defined at specific level in stalagmite from cave in northeastern Indian state.
Meghalayan Age was part of longer period known as Epoch, which reflects everything that has happened over past 11,700 years. It began with mega global drought that devastated ancient agricultural civilisations from Egypt to China. This age is unique because it is first interval in Earth’s geological history that coincided with major cultural event, as agricultural societies struggled to recover from shift in climate.
The droughts over 200-year period had resulted in human migrations in Egypt, Syria, Palestine, Mesopotamia, Greece, Indus valley and Yangtze river valley. The change in global climate during Meghalayan Age was likely triggered by shifts in ocean and atmospheric circulation.
Middle Holocene Northgrippian Age and Early Holocene Greenlandian Age: These two ages are defined with beginnings at climatic events that happened about 8,300 years and 11,700 years ago, respectively. The lower boundary of Greenlandian and Northgripppian stages are defined at specific levels in Greenland ice cores. The ice cores are now identified as international geostandards, and have been placed in protected archives accessible for further study.
Geologists divide 4.6-billion-year existence of Earth into distinct periods. Each period corresponds to significant events such as break-up of continents, shifts in climate, and emergence of particular types of animals and plant life. These units of geologic time scale are based on sedimentary strata that have accumulated over time and contain within them sediment types, fossils and chemical isotopes that record passage of time as well as physical and biological events that produced them. Those intervals of sedimentary strata on which ages are based are referred to as stages.